Zobrazeno 1 - 10
of 29
pro vyhledávání: '"Xiuxiang ZHU"'
Publikováno v:
Cell Death and Disease, Vol 15, Iss 9, Pp 1-14 (2024)
Abstract Circular RNAs (circRNAs) are a type of regulatory RNA that feature covalently closed single-stranded loops. Evidence suggested that circRNAs play important roles in the progression and development of various cancers. However, the impact of c
Externí odkaz:
https://doaj.org/article/cb692b15ffbd4afdb0827c13c9e7e51d
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-13 (2024)
Abstract This study aimed to evaluate the potential of capping protein (actin filament) muscle Z-line subunit β (CAPZB) messenger ribonucleic acid (mRNA) levels as a biomarker for distinguishing low-grade squamous intraepithelial lesions of the cerv
Externí odkaz:
https://doaj.org/article/7c1830d92cca476c94e3dc5de1ab75d9
Publikováno v:
Shiyou shiyan dizhi, Vol 45, Iss 2, Pp 327-337 (2023)
By 2D gas chromatography and time-of-flight mass spectrometry (GC×GC-TOFMS), 81 ethanodiamondoids with 1-3 cages were detected quantitatively in Ordovician crude oil from well SN1, Shuntuoguole area, Tarim Basin, including 47 ethanoadamantanes with
Externí odkaz:
https://doaj.org/article/9b283ea58b834fa88ac2fe168246c83e
Publikováno v:
Shiyou shiyan dizhi, Vol 44, Iss 4, Pp 677-686 (2022)
Three sections of fracture-cave filling bitumen with a total thickness of approximately 3.25 m were discovered between 7 265 m and 7 275 m in Ordovician Yijianfang Formation micrites in the well SHB1-X-3, Shunbei No.1 fault zone, central Tarim Basin.
Externí odkaz:
https://doaj.org/article/c43cfc523b2d47eda3895078d21949c6
Publikováno v:
Shiyou shiyan dizhi, Vol 44, Iss 3, Pp 402-412 (2022)
The types and properties of the ultra-deep Ordovician oil and gas resources in the strike-slip fault zone of the Shunbei oil and gas field in the Tarim Basin show regular changes. The main controlling factors of oil and gas distributional characters
Externí odkaz:
https://doaj.org/article/9b6394ac4437494ea05bd0724c6630d5
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
As a gas-rich region in the Tarim Basin, the northern Shuntuoguole area (also known as the Shunbei area) is an attractive prospect. Non-etheless, the debate about the origins of these natural gas continues. The analysis on the geological context, nat
Externí odkaz:
https://doaj.org/article/37e31a0a4b6a482d9e9dc3d105c64b7f
Autor:
Anlai Ma, Zhiliang He, Lu Yun, Xian Wu, Nansheng Qiu, Jian Chang, Huixi Lin, Zicheng Cao, Xiuxiang Zhu, Donghua You
Publikováno v:
Journal of Natural Gas Geoscience, Vol 6, Iss 5, Pp 289-300 (2021)
Ultra-deep Ordovician in Shuntuoguole area, Tarim Basin, NW China, has complex oil & gas phases, in which light oil, volatile oil, condensate and dry gas phases coexisting. The study compares the geochemical characteristics and origin of Ordovician u
Externí odkaz:
https://doaj.org/article/bff2bd48143148b385b81789608909b1
Publikováno v:
Shiyou shiyan dizhi, Vol 43, Iss 5, Pp 818-825 (2021)
With the expansion to the deep strata for the exploration of marine oil and gas in the Tarim Basin, the upper limit of temperature for the occurrence of ultra-deep reservoirs has become a scientific concerning of organic geochemistry and petroleum ge
Externí odkaz:
https://doaj.org/article/b57e5a5dcac8413fa0cdcf277fc10e45
Publikováno v:
Shiyou shiyan dizhi, Vol 43, Iss 4, Pp 648-654 (2021)
Exploration experiences have showed that the main source rocks of the Lower Cambrian have not been developed in the Bachu uplift; however, the well MB1 in this area had a good oil and gas showing in the Lower Cambrian.To clarify the hydrocarbon sourc
Externí odkaz:
https://doaj.org/article/368a45b891c64db69e8b9318edb22955
Publikováno v:
Journal of Natural Gas Geoscience, Vol 6, Iss 2, Pp 89-99 (2021)
The ultra-deep Ordovician Yijianfang-Yingshan Formations from the North Shuntuoguole region in Tarim Basin, NW China, have produced industrial oil and gas. The reservoir fluid phases differed between faults. Using the GG-MS and GC × GC-TOFMS methods
Externí odkaz:
https://doaj.org/article/b0dcd6f6d53d4b208626f6fc3a14aa1a